Affiliation:
1. Analytical Center, Tagansky District, 115035 Moscow, Russian Federation
Abstract
The study investigated geomorphology of the Japan Trench located east of Japan, Pacific Ocean. A high-resolution GEBCO
Gridded Bathymetric Dataset was used for modeling, mapping and visualization. The study aimed to compare and analyse variations in the geomorphic
structures of the two parts of the trench and to visualize variations in the geological, geophysical and bathymetric settings. Technically, the
cartographic work was performed using scripting based on the Generic Mapping Toolset (GMT). Modelled cross-sectioning orthogonal profiles transecting
the trench in a perpendicular direction were automatically digitized and graphed in the two segments. The results of the bathymetric analysis shown
that the southern part is shallower: with deeper values in absolute (139 samples between –7000 to –8000 m) and statistical records (the most frequent
values are within –5500 to –5800 m) comparing to the northern segment (–5300 to –5500 m). The geomorphological analysis shows a more complicated relief
in the northern part of the trench, which has a higher seismic activity. The southern part has a gentler slope on the Honshu island side. The geoid
modeling along the trench ranges in 0–20 mGal. The highest values are recorded by the Honshu Island (>40 mGal). The rest of the area has rather
moderate undulations (20–40 mGal). The free-air marine gravity of the Sea of Japan is <40 mGal. The results include 2D and 3D graphical models,
thematic cartographic maps, spatial and statistical analysis of the Japan Trench geomorphology. Tested GMT functionality can be applied to future
regional bathymetric modeling of the ocean trenches. All presented maps and graphs are made using GMT scripting toolset.
Publisher
Vilnius Gediminas Technical University
Subject
General Earth and Planetary Sciences
Cited by
23 articles.
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